2022
DOI: 10.1134/s0097807822050141
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The Carbonate System of the Estuaries of the Syran and Ul’ban Rivers (Ul’banskii Bay, the Sea of Okhotsk) during Spring Flood

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Cited by 5 publications
(1 citation statement)
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“…The obtained concentrations are comparable with the NO − 3 concentrations in anthropogenically polluted rivers; for example, in the Razdolnaya River flowing across an urbanized area in China and Russia (NO − 3 range is 10-30 µmol/L in the high water period and up to 300 µmol/L in the low water period) [51]; in Japanese rivers subjected to anthropogenic nitrate flux (NO − 3 range is 18-55 µmol/L) [52]; and in small rivers in China with anthropogenic effluents (NO − 3 range is 15-368 µmol/L) [53]. At the same time, the NO − 3 concentrations are much lower (0.02-0.37 µmol/L in the high water period) in the Sea of Okhotsk rivers not exposed to anthropogenic loads and volcanic activities [54].…”
Section: River Feeding Sources and Nutrient Fluxes With River Runoffmentioning
confidence: 99%
“…The obtained concentrations are comparable with the NO − 3 concentrations in anthropogenically polluted rivers; for example, in the Razdolnaya River flowing across an urbanized area in China and Russia (NO − 3 range is 10-30 µmol/L in the high water period and up to 300 µmol/L in the low water period) [51]; in Japanese rivers subjected to anthropogenic nitrate flux (NO − 3 range is 18-55 µmol/L) [52]; and in small rivers in China with anthropogenic effluents (NO − 3 range is 15-368 µmol/L) [53]. At the same time, the NO − 3 concentrations are much lower (0.02-0.37 µmol/L in the high water period) in the Sea of Okhotsk rivers not exposed to anthropogenic loads and volcanic activities [54].…”
Section: River Feeding Sources and Nutrient Fluxes With River Runoffmentioning
confidence: 99%